KMS Institute of Mountain Hazards and Environment,CAS
|Alternative Title||NEOTECTONICS IN CARPATHIANS REGION (ROMANIA) AND CORRELATION WITH HENGDUAN MOUNTAINS REGION|
|Keyword||新构造 喀尔巴阡山地区 横断山地区|
The obvious features of neotectonics in Carpathians region are mainly characterized by the development ofthe mountain area and also the downwarping at the foot of mountain. After Wallachian orogeny , the region was upheaved and folded , the regression took place at the end of Late Neogene , and since then occupied by lacustrine deposits with transgression locally existed. During Quaternary , the most obviously uplifting area is from east Carpathians to south Carpathians , lifting more than 1000m; while relative subsidence occurred in Romania depression and Hungary depression at both sides of the mountains , with 2000- 2500m of deposits piled up in Romania depression. Total range between uplifting and subsidence can reach up to 3000 - 3500m; but there isn' t any obvious change in Dobrogean and Moldova platform. The strong downwarping at the front of Mt. Carpathians and the obvious folds of N2-Q1 indicated that a NW - SE horizontal compression do exist , and it still keeps on the compression , which was supported by the ground deformation measurement and the anelyses to macroseisms and volcanoes. From all above , the uplifting of Mt. Carpathians is supposed to related with such compression , especially when "Black Sea microplate" subduction to Carpathians.
The Carpathians and Hengduan mountain system all belong to neotectonic orogenic belt; both of them have the same neotectonic period , and during the late period , the rate of vertical and horizontal movement began to accelarate in both areas. As a whole , the develop ments of neotectonics in both regions are similar. But compared with the Carpathians , Hengduan mountain system which occupied a special tectonic position is morè complex in tectonic strength , type and evolution , and also left more plentiful resources and more complicated environmental problems.
|陈富斌. 喀尔巴阡山地区（罗马尼亚）的新构造及其与横断山地区的对比. 横断山系新构造研究. 成都:成都地图出版社,1992:93-105.|
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